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Warm afterglow from the Toarcian Oceanic Anoxic Event drives the success of deep-adapted brachiopods
Many aspects of the supposed hyperthermal Toarcian Oceanic Anoxic Event (T-OAE, Early Jurassic, c. 182 Ma) are well understood but a lack of robust palaeotemperature data severely limits reconstruction of the processes that drove the T-OAE and associated environmental and biotic changes. New oxygen...
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| Vydáno v: | Sci Rep |
|---|---|
| Hlavní autoři: | , , , , , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group UK
2020
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7162941/ https://ncbi.nlm.nih.gov/pubmed/32300235 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-020-63487-6 |
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